ti s
s th infl e s lum rn Hem te vari proxy to explain the orbital control on advances and retreats of the NH ice sheets. According to the theory, changes in high-latitude summer insolation are the main control on ice sheet expansion and This discrepancy betweenMilankovitch theory and the global ice volu...
Other Authors: | |
---|---|
Format: | Text |
Language: | English |
Subjects: | |
Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.612.2715 http://www.earth.lsa.umich.edu/paleoclimate/pdfs/lee_poulsen_qsr_2009.pdf |
id |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.612.2715 |
---|---|
record_format |
openpolar |
spelling |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.612.2715 2023-05-15T16:40:35+02:00 ti s The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.612.2715 http://www.earth.lsa.umich.edu/paleoclimate/pdfs/lee_poulsen_qsr_2009.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.612.2715 http://www.earth.lsa.umich.edu/paleoclimate/pdfs/lee_poulsen_qsr_2009.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.earth.lsa.umich.edu/paleoclimate/pdfs/lee_poulsen_qsr_2009.pdf text ftciteseerx 2016-01-08T14:34:05Z s th infl e s lum rn Hem te vari proxy to explain the orbital control on advances and retreats of the NH ice sheets. According to the theory, changes in high-latitude summer insolation are the main control on ice sheet expansion and This discrepancy betweenMilankovitch theory and the global ice volume record has been coined the ‘‘41 kyr problem’ ’ (Raymo and Nisancioglu, 2003). The prevalence of the obliquity signal in the Pleistocene global ice volume record has been attributed to factors including the state of the tropical Pacific Ocean (Philander and Fed- Text Ice Sheet Unknown Pacific |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
s th infl e s lum rn Hem te vari proxy to explain the orbital control on advances and retreats of the NH ice sheets. According to the theory, changes in high-latitude summer insolation are the main control on ice sheet expansion and This discrepancy betweenMilankovitch theory and the global ice volume record has been coined the ‘‘41 kyr problem’ ’ (Raymo and Nisancioglu, 2003). The prevalence of the obliquity signal in the Pleistocene global ice volume record has been attributed to factors including the state of the tropical Pacific Ocean (Philander and Fed- |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
title |
ti s |
spellingShingle |
ti s |
title_short |
ti s |
title_full |
ti s |
title_fullStr |
ti s |
title_full_unstemmed |
ti s |
title_sort |
ti s |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.612.2715 http://www.earth.lsa.umich.edu/paleoclimate/pdfs/lee_poulsen_qsr_2009.pdf |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
http://www.earth.lsa.umich.edu/paleoclimate/pdfs/lee_poulsen_qsr_2009.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.612.2715 http://www.earth.lsa.umich.edu/paleoclimate/pdfs/lee_poulsen_qsr_2009.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766030981334040576 |